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Effects of Cloud on Land Surface Temperature (LST) Change in Thermal Infrared Remote Sensing Images: a Case Study of Landsat 8 Data

机译:云对热红外遥感图像陆地温度(LST)变化的影响 - 以兰德拉德8数据为例

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Clouds exert a great influence on land surface temperature (LST). It remains unclear how clouds affect the LST change in satellite images. The focus of the study is to examine the effects of cloud on LST change in Landsat 8 images over various ground surface types, cloud sizes and seasonal scales. The difference between solar and satellite geometry over the images provides the possible way to identify the impact of cloud in Landsat 8 images. The shadow of cloud represents the true effects of cloud on LST change. Using the available mono-window algorithm, we were able to retrieve the LST of the shadow for the analysis of the cloud effects. Four typical ground surfaces were selected for the analysis: desert/bare surface, vegetation, urban and water covered area. The LST difference between the shadow and its nearby clear-sky region represents the effects of cloud on LST change in the corresponding ground surface. The results indicated that the, highest LST difference was observed over dessert/barren land in the magnitude of 8.28°C. Moreover, when the cloud size relatively smaller or larger the effect on LST slightly varies. The summer season has the most remarkable effect of cloud on LST change. The water surface has the lowest LST difference in overall cloud analysis. These change of LST under cloud in various conditions can be helpful for the studies which are focus on LST estimation during cloudy conditions.
机译:云对陆地温度(LST)产生了很大的影响。仍然不清楚云如何影响卫星图像的LST变化。该研究的重点是研究云对各种地面类型,云尺寸和季节性尺度的Landsat 8图像中LST变化的影响。在图像上的太阳能和卫星几何形状的差异提供了识别云在Landsat 8图像中的影响的可能方法。云的阴影是云对LST变化的真实影响。使用可用的单窗算法,我们能够检索阴影的LST,以分析云效果。选择四个典型的地面用于分析:沙漠/裸露的表面,植被,城市和水覆盖区域。阴影和附近的清晰天空区域之间的LST差异表示云对相应地面的LST变化的影响。结果表明,在8.28°C的幅度下观察到甜点/贫瘠陆上最高的LST差异。此外,当云尺寸相对较小或更大时,LST的效果略微变化。夏季对LST变化的云具有最显着的影响。水面具有整体云分析中最低的LST差异。在各种条件下云下的LST的这些变化可能有助于在多云条件下专注于LST估计的研究。

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